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Effect of Free-fall Nozzle Channel Dispersion Angle on TC4 Discontinuous Droplets Pre-breakup in EIGA
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作者 邹海平 LI Fenglei +1 位作者 NGAI Tungwai XIAO Zhiyu 《Journal of Wuhan University of Technology(Materials Science)》 SCIE EI CAS CSCD 2023年第1期171-183,共13页
The effect of the inlet gas pressure,supplementary gas pressure and nozzle channel dispersion angle on the pre-breakup behavior of Ti-6Al-4V(TC4)discontinuous droplets during EIGA was investigated by combining numeric... The effect of the inlet gas pressure,supplementary gas pressure and nozzle channel dispersion angle on the pre-breakup behavior of Ti-6Al-4V(TC4)discontinuous droplets during EIGA was investigated by combining numerical simulation with experiments.The results show that the axial velocity at the recirculation zone before the stagnation location was first increased and decreased then increased significantly after the peak value,while the pressure of the recirculation zone increased with the increase in inlet pressure.With the supplementary pressure increasing,the velocity magnitude and range of the recirculation zone gradually decreased.As the dispersion angle of the nozzle channel increased,the pre-breakup efficiency of droplets gradually decreased,but the adhesion phenomenon of droplets on the inner wall surface of the nozzle channel(IWSNC)gradually weakened.Under the inlet pressure of 4 MPa,a supplementary pressure of 0.05 MPa,and the dispersion angle of 15°,the uniform and spherical TC4 powders with diameter of 70μm were prepared,which was consistent with the simulation results.The optimized process parameters is a balance between the size of the pre-atomized particles and the back-spraying and bonding phenomenons of droplets. 展开更多
关键词 discontinuous droplets dispersion angle numerical simulation pre-breakup EIGA
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梵净山区新元古界下部喀斯特不整合的确认及其地质意义 被引量:3
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作者 张慧 陈明华 +2 位作者 彭成龙 蒋开源 于宁 《贵州地质》 2005年第4期221-223,228,共4页
本文描述了梵净山区新元古界下部乌叶组与甲路组之间的喀斯特不整合的空间分布、地质特征,从而进一步确认了它的存在;指出该不整合是格林威尔碰撞造山之后强烈隆升的产物,代表了Rod inia超大陆在新元古代裂解前地壳经历的隆起并遭受剥... 本文描述了梵净山区新元古界下部乌叶组与甲路组之间的喀斯特不整合的空间分布、地质特征,从而进一步确认了它的存在;指出该不整合是格林威尔碰撞造山之后强烈隆升的产物,代表了Rod inia超大陆在新元古代裂解前地壳经历的隆起并遭受剥蚀侵蚀的历程,从而对研究该时期地层的空间变异、沉积环境,特别是探讨Rod inia超大陆岩相演化都具有重要的科学意义。 展开更多
关键词 喀斯特不整合 新元古界下部 裂前隆起 RODINIA超大陆 梵净山 贵州
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